Left Fork Dome Creek

The Left Fork Dome Creek is a gold mine located in Alaska.

About the MRDS Data:

All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.

Mine Info

Name: Left Fork Dome Creek

State:  Alaska

County:  na

Elevation:

Commodity: Gold

Lat, Long: 64.88611, -164.65111

Map: View on Google Maps

Satelite View

MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.


Satelite image of the Left Fork Dome Creek

Left Fork Dome Creek MRDS details

Site Name

Primary: Left Fork Dome Creek


Commodity

Primary: Gold


Location

State: Alaska
District: Kougarok; Iron Creek


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Years of Production:
Organization:
Significant:


Physiography

Not available


Mineral Deposit Model

Model Name: Placer Au-PGE


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Gold


Comments

Comment (Workings): Workings / Exploration = Extensive, small-scale placer mining was carried out on this creek by 1908.

Comment (Exploration): Status = Probably inactive

Comment (Reference): Primary Reference = Smith, 1909

Comment (Deposit): Model Name = Placer Au-PGE (Cox and Singer, 1986; model 39a).

Comment (Geology): Geologic Description = Most of the lower parts of Left Fork Dome Creek were placer mined during the first few years of mining in the area. Production was estimated to be about $20,000 or almost 1,000 ounces of gold by 1908 (Smith, 1909). Surface water was lost to underground channels (karst ?) in the marble of bedrock. Bedrock rock is part of a lower Paleozoic metasedimentary assemblage (Till and others, 1986).

Comment (Geology): Age = Quaternary.


References

Reference (Deposit): Smith, P.S., 1909, Recent developments in southern Seward Peninsula: U.S. Geological Survey Bulletin 379-F, p. 267-301.

Reference (Deposit): Till, A.B., Dumoulin, J.A., Gamble, B. ., Kaufman, D.S., and Carroll, P.I., 1986, Preliminary geologic map and fossil data, Soloman, Bendeleben, and southern Kotzebue quadrangles, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 86-276, 10 p., 3 plates, scale 1:250,000.

Reference (Deposit): Cobb, E.H., 1978, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Solomon quadrangle, Alaska: U.S. Geological Survey Open-File Report 78-181, 185 p.

Reference (Deposit): Cobb, E.H., 1972, Metallic resources map of the Solomon quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-445, scale 1:250,000.


The Top Ten Gold Producing States

The Top Ten Gold Producing States

These ten states contributed the most to the gold production that built the West from 1848 through the 1930s. The Top Ten Gold Producing States.